Pressure range of
in situ x-ray observation has been extended very close to 100 GPa, by interfacing the Kawai-type multi-anvil apparatus (KMA) equipped with sintered diamond anvils with the synchrotron radiation at SPring-8. High-pressure phase equilibria in Fe
2O
3 and MgGeO
3 are summarized. Isostructural reduction in electrical resistance of hematite by three orders of magnitude at pressures 54-56 GPa strongly suggests the occurrence of a Mott transition. In MgGeO
3, special attention was paid to the d
P/d
T slope of the phase boundary between perovskite and post-perovskite phases. Spin transition of Fe
2+ in (Mg
0.83Fe
0.17)O is also briefly reported.
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